In the article the featuresof the formationandmetallogenyof the geologicalstructuresofGreatAltai (RudnyAltai, Kalba-Narym, WesternKalbaandJarma-Saur) whichareincludedinto the systemoftheCentralAsianmobilebeltareconsidered. The
characteristic of the main types of rare metal minefields of the Kalba-Narymsky
belt genetically connected with the Perm granitoid magmatism of the
post-conflict orogenny stage of activization is given. The rhythmical and
pulsation model of pegmatitovy ore formation in the conditions of the
half-closed magmatic system, reflecting the phasic development of mineral complexes
from graphic and oligoclase-microcline (barren) to microcline-albite and
albite-spodumene ore (Ta, Nb, Be, Li, Sn, etc.) is developed. On the basis of
the revealed criteria of ore formation recommendations about the direction of
the further researches are made.
Cite this paper
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